supported by the National Natural Science Foundation of China (Grant Nos.42272053 and 41930215);the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources (Grant No.MSFGPMR2022-6)。
Refractory lithospheric deep roots are the cornerstone for the prolonged stability of cratons and mantle xenoliths are normally the key targets for study on the evolution of such deep roots. In regions with few mantle...
supported by the National Natural Science Foundation of China(42074106 and 91962110);the National Key R&D Plan of China(2023YFF0803302).
The phase of secular evolution of continents is manifested as the degree of compositional differentiation,modification and maturation of continental crusts,which is vital in understanding the mechanism of continental ...
supported by the National Natural Science Foundation of China (Grant Nos. 41630209, U2039203, 42130306)。
Cratons formed due to the specific melting regime of the primitive mantle with elevated mantle temperature during Archean.However,each craton has undergone a distinct evolution history,and some have lost their stabili...
supported by the DREAM project of the National Key R&D Program of China(No.2016YFC0600402);the National Natural Science Foundation of China(No.41774071);the US Gelogical Survey Earthquake Hazards Program。
We present crustal models for seismic P-waves(Vp),S-waves(Vs)and the Vp/Vs ratio across the southern North China Craton along latitude 36°N.Our results are based on inverse and forward modeling of long-range wide-ang...
supported by the National Key R&D Program of China(Grant No.2016YFC0600109);the National Natural Science Foundation of China(Grant Nos.41725014&41688103)。
The Archean mantle lithosphere beneath the North China Craton(NCC)was transformed in the Mesozoic,leading to the craton destruction.Despite the significant breakthroughs in the craton studies,lithospheric transformati...
The 2020 TKK Science Award in Earth Sciences was conferred on CAS Member Prof.ZHU Rixiang,a researcher working at the CAS Institute of Geology and Geophysics,for his outstanding work on the destruction of the North Ch...
supported by the Ministry of Science and Technology of People’s Republic of China(Grant No.2016YFC0600109);the National Natural Science Foundation of China(Grant No.41688103).
It is well known that the destruction of the North China Carton(NCC)is closely related to subduction of the Paleo-Pacific slab,but materials recording such subduction has not been identified at the peak time of decrat...
National Key R&D Program of China(2016YFC0600408);Strategic Priority Research Program(B)of the Chinese Academy of Sciences(XDB18020102);Guangdong Natural Science Funds(2014A030306032 and 2015TQ01Z611);Youth Innovation Promotion Association CAS(2016315)。
The mechanism of lithospheric removal and destruction of the North China Craton(NCC)has been hotly debated for decades.It is now generally accepted that the subduction of the(Paleo)-Pacific plate played an important r...
supported by the National Natural Science Foundation of China(grants No.41872194,41872203)
Objective Early Precambrian rocks are widely distributed in the khondalite series belt of the North China Craton(NCC),and previous studies have shown that the metamorphic ages of^2.5 Ga and^1.95 Ga are widespread.
supported by the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (No. MSFGPMR16);the Key Program of the Ministry of Land and Resources of China (No. 1212011220497)
Archean high-K granitoids, generally formed after tonalite-trondhjemite-granodiorite (TTGs), are important for understanding crustal reworking of ancient cratons. The Linshan Archean high-K granitoids from the souther...